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Water Quality Status of Kipawa Lake and Kipawa River

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Water Quality Status of Kipawa Lake and Kipawa River Water Quality Status of Kipawa Lake and Kipawa River By: Christina Moreau Kipawa Lake Preservation Society P.O. Box 1 Temiscaming Quebec J0Z 3R0 www.kipawalakepreservationsociety.ca [email protected] © 2016 Introduction Kipawa Lake is a large, oligotrophic, Canadian shield lake located in the South-West portion of the Province of Quebec (Figure 1). With the exception of a few locations (Kipawa, Laniel, etc.) the lake is fairly undeveloped and sparsely populated. Much of the area is undisturbed wilderness and attracts tourists and visitors from Quebec, Ontario and the United States who hunt, fish, canoe, kayak or participate in other outdoor activities. There are over 25 fish species that have been identified in Kipawa Lake and its tributaries including Brook Trout Salvelinus fontinalis, Yellow Perch Perca flavescens, Brown Bullhead Ameiurus nebulosus, Cisco Coregonus artedi, Lake Whitefish Coregonus clupeaformis , Burbot Lota lota, White Sucker Catostomus commersoni, Golden Shiner Notemigonus crysoleucas, Smallmouth Bass Micropterus dolomieu, Northern Redbelly Dace Phoxinus eos, etc. The main sportfish are Walleye Sander vitreus, Northern Pike Esox lucius and Lake Trout Salvelinus namaycush. Kipawa Lake is thought to have good water quality and it is used as a source of drinking water for many nearby communities (OBVT 2014). Moreau (2005) indicated that the phytoplankton composition present at Edward’s Narrows in 2004 were representative of a pristine environment - good water quality status and free of organic pollution. However, the study was conducted in a remote lake section with little cottage development. In recent years, organic pollution is thought to have occurred in more populated lake sections as blooms of cyanobacteria (blue-green algae) were reported near Kipawa in 2012 and near Laniel in 2013 (MDDELCC 2015). Additionally, there have been complaints of deteriorating water quality in certain lake sections (OBVT 2014). Fish tissues were analyzed for metals (mercury, arsenic, selenium, barium, cadmium, chromium, cobalt, copper, iron, manganese, molybdenum, nickel, lead, strontium, uranium, vanadium and zinc), PCBs (polycholorinated biphenyls), PBDEs (Polybrominated diphenyl ethers), dioxins and furans in 2010/2011 by the Quebec Ministry of Sustainable Development, Environment, Wildlife and Parks. Mercury levels were found to exceed acceptable levels (>0.5 mg/kg) in both Lake Trout and Walleye. All other metals were found to be within normal range 1 | P a g e with the exception of arsenic which was elevated in Lake Trout compared to reference regions. PCBs, PBDEs, dioxins and furans were low in Lake Trout tissues analyzed (OBVT 2014). To date, there is a lack of published information regarding the water quality of Kipawa Lake and its tributaries. To our knowledge phosphate levels, metals and other pollutants have yet to be analyzed in any location in the watershed. No baseline data exists regarding water quality of the upper Kipawa River (Sairs (formerly Brennan) Lake to Red Pine Chutes) and yet a rare earth mine is proposed for development in this region. Given that this area acts as important spawning habitat for Walleye, Lake Trout, Brook Trout, Northern Pike, Yellow Perch and other fish species, we felt it vital that current water quality status be determined including analysis of the level of metals as well as dissolved ions and other water quality parameters. This data will help establish a baseline and point of reference for water quality in this region which is crucially important should proposed development plans proceed. Methods On August 16th 2015 ‘grab’ water samples were collected at the surface from a site along the upper Kipawa River (near Lake Sheffield; 46°48’27.78”N, 78°31’0.18”W; Figure 1 and 2). Samples were stored in a cooler with ice packs and transported to North Bay ON for shipment to laboratories within 24-48 hours. Testmark Laboratories in Garson ON provided analysis of the level of metals, dissolved ions, pollutants and other water quality parameters. Becquerel Laboratories in Mississauga ON provided analysis of gross alpha and gross beta radiation levels. August results showed an elevated level of aluminum and copper, therefore testing of metals and pH were repeated with 3 replicates on October 4th 2015. Due to low water levels and strong current along the river, sampling at the original site was not possible and samples were instead collected a few kilometers downstream at Red Pine Chutes (46°50’23.45”N, 78°36’45.70”W; Figure 2). Samples were transported to North Bay, ON and shipped to Testmark Laboratories in Garson ON within 24 – 48 hours of collection. 2 | P a g e In addition to collection of samples, dissolved oxygen and temperature readings were obtained at sample locations (Kipawa River 46°48’27.78”N, 78°31’0.18”W and Red Pine Chutes 46°50’23.45”N, 78°36’45.70”W) as well as at a few nearby sites: Lake Sheffield (46°48’7.78”N, 78°30’58.75”W), Long Narrows (46°50’47.84”N, 78°39’18.35”W) and Grindstone/Mungo Bay (46°47’54.03”N, 78°40’38.91”W). Dissolved oxygen and temperature readings were measured at one meter intervals from the surface to the maximum depth at sample location using a handheld YSI dissolved oxygen and temperature meter. Figure 1. Map of Kipawa Lake, Quebec. Sampling occurred in the south-east arm of the lake (Grindstone and Long Narrows) as well as along the Kipawa River (Red Pine Chutes and Lac Sheffield). Circles indicate sites where only dissolved oxygen and temperature profiles were obtained while squares indicate sites where dissolved oxygen and temperature profiles were obtained in addition to testing for metals, pH and other water quality parameters. 3 | P a g e Figure 2. Map of the Kipawa watershed with a close up view of sampling sites used for water quality testing conducted in 2015. Sampling occurred in the south-east arm of the lake (Grindstone and Long Narrows) as well as along the Kipawa River (Red Pine Chutes and Lake Sheffield). Circles indicate sites where only dissolved oxygen and temperature profiles were obtained while squares indicate sites where dissolved oxygen and temperature profiles were obtained in addition to testing for metals, pH and other water quality parameters. Results Dissolved oxygen and temperature - On August 16th surface temperatures were quite warm (25°C) and there was evidence of a weak thermocline with temperature decreasing slightly with depth (Figure 3 and 4). At the Kipawa River sample site dissolved oxygen was approximately 7 mg/L at all depths (Figure 4) while at a second site on Lake Sheffield dissolved oxygen was fairly low (5.3 – 5.7 mg/L) from the surface to a depth of 4 meters, increased slightly (7.19 – 8.57 mg/L) from 4 to 9 meters and then decreased drastically to 4 mg/L at depth (Figure 3). 4 | P a g e On October 4th, surface temperatures had cooled significantly to approximately 15°C. Temperature and dissolved oxygen were fairly consistent with depth at Red Pine Chutes and Long Narrows, with a well-mixed water column and the absence of thermal stratification. Temperature was consistently around 15°C and dissolved oxygen was fairly elevated (8.5 - 10.2 mg/L) even at depth (Figure 5 and 6). Lake Grindstone (Mungo Bay) on the other hand, showed a significant decrease in temperature as well as dissolved oxygen at depth. From 12 to 14 meters the dissolved oxygen concentration dropped rapidly from 9.16 to 5.84 mg/L and continued to decrease with depth to 5.69 mg/L at 17 meters (Figure 7). While previous studies (Nadeau and Trudeau 2012; Moreau 2016) have reported elevated dissolved oxygen even at depth for Kipawa Lake, we observed a few areas where dissolved oxygen was quite low at depth and below ideal levels for the protection of aquatic life. On August 16th 2015 at Lake Sheffield we observed hypoxic (low oxygen) conditions at depth with values of 4 mg/L at a temperature of 16°C (Figure 3). This value is below the minimum required to support both cold water species (6 mg/L) and warm water species (5mg/L). Similarly, on October 4th 2015 at Lake Grindstone low oxygen (5.69 – 5.84 mg/L) was observed at depths of 14-18 meters and at temperatures of 12°C (Figure 7). This is below the level needed for cold water species (6 mg/L) and near the lower limit required for warm water species (5 mg/L; Table 1; Ontario Ministry of Environment and Energy 1994). It is important to note that oxygen concentrations vary considerably on a seasonal basis as well as on a daily basis. Time of day can have a large impact on oxygen levels, all aquatic organisms respire consuming oxygen while only primary producers (e.g. phytoplankton and aquatic plants) carryout photosynthesis producing oxygen. Often dissolved oxygen is lowest in the early morning hours as respiration occurs overnight however photosynthesis and the production of oxygen can only occur in the presence of sunlight – during daylight hours. Furthermore, dissolved oxygen concentrations vary considerably with location in the water column, near the surface oxygen is typically higher due to wave action and mixing with the atmosphere. Similarly, the first few meters where light is able to penetrate is generally higher in oxygen due to the presence of photosynthetic organisms that produce oxygen. In contrast, at depth photosynthesis does not occur due to a lack of available light, however respiration does take 5 | P a g e place consuming oxygen. Microbes, usually found in bottom sediments, also consume oxygen during the decomposition of organic matter. The input of large amounts of organic matter (e.g.
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